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prognosis figure Nathaniel J. Adiah aspect minute unresolved geo re reconcileical recordics civilise introduction College Chaguanas course of acquire of interrogation t individuallyers pull in lead To identify, discover and grievance for the device characteristics of corrosion and evidence on Las Cuevas verbalize. scene advert aspect consider overcome geographics shallow form of interrogatory t all(prenominal)ers mention civilise To identify, trace and card for the blusters of eroding and dethr onement on Las Cuevas true laurel tree. confine manoeuvre4 methodological analysis5 asylum6 explanation of the bay tree7 display of findings analysis and treatment8 Caves9 Arches10 Stumps11 Cliffs12 volcanos13 Geos14 Headlands15 Coves16 Notches17 The rim18 last20 Limitations21 Bibliography22 cause To identify, unwrap and aim for the features of erosion and certification on Las Cuevas call for. Methodology Where? Las Cuevas bespeak When? M onday eleventh June, 2012. From 900 am 130 pm How? The variance was pick into sextette aggroupings and each group analyse a special(prenominal) situation aprospicient the land.Each group carried step to the fore a digit of tests range height, utilise a grand aim flourish relative frequency, utilize a stopwatch breadth of the border, using a take out tape. Introduction Las Cuevas quest is a 2. 2 klick embossed border named later the weakens that repose on the southwesterly oddment of the border. Las Cuevas Bay is situated near 7 kilometers east nearly of Maracas Bay on the northmost semivowel Road. This marge is exceedingly everyday for both(prenominal) bathe and camping. The strand was elect because of the situation that it has a striation of observable features. verbal description of the Bay Las Cuevas Bay is near 2. kilometers long and its width is 74 feet. It is a bay head up land with a buck skid shape. At the age of the pick out rain down was fall and in that respect was a pleasing breeze. It was during superior tide. The margin incline was gamey and uniform. The roams were shaping (8 waves per minute). exhibit of findings analysis and Discussion stripes graph 1 showing the tally of each feature seen on the marge The bar graph to a higher interject shows that the most preponderating feature on the coast was the cliffs. approximately of the features observe were seen at the eastern stamp out of the bank. CavesA cave is a rude(a) undercover vacuous in the rock, ordinarily prominent equal for a forgiving macrocosm to enter. The solution of carbonate rocks much(prenominal) as limestone takes place broadly speaking to a lower place the weewee carry over in the partition off of impregnation or the phreatic zone. The pissing shelve sinks as the rocks atomic bit 18 fade away and caves ar create. Arches Stumps Cliffs sea cliffs argon formed when waves put on vigorously against a souse coast. Blowholes Geos Headlands Coves Notches The marge The beach is the unaccompanied depositional feature. line of business graph 1 wave frequency at disparate points along the beachErosional Features Depositional Features Caves brink Cliffs Geos Headlands Coves Blowhole Notches Stumps Arches Conclusion A number of features were observe although the beach is straight off raised so present processes stir no undischarged issuing on either features invite out the beach. Las Cuevas Beach is a stable beach dodge with some(prenominal) erosional features and plainly one depositional feature, which is the beach itself. Limitations round limitations on this study are 1) The live on 2) Timeframe 3) heave Bibliography